{"id":12057,"date":"2017-03-15T14:52:29","date_gmt":"2017-03-15T13:52:29","guid":{"rendered":"http:\/\/karmaka.de\/?p=12057"},"modified":"2017-03-15T14:54:15","modified_gmt":"2017-03-15T13:54:15","slug":"a-high-spatial-resolution-synchrotron-mossbauer-study-of-the-tazewell-iiicd-and-esquel-pallasite-meteorites","status":"publish","type":"post","link":"https:\/\/karmaka.de\/?p=12057","title":{"rendered":"A high spatial resolution synchrotron M\u00f6ssbauer study of the Tazewell IIICD and Esquel pallasite meteorites.<span class=\"badge-status\" style=\"background:#787878\">OPEN ACCESS<\/span>&nbsp;"},"content":{"rendered":"<p>Blukis, R., R\u00fcffer, R., Chumakov, A. I. and Harrison, R. J.<\/p>\n<p>Meteorit Planet Sci. doi:10.1111\/maps.12841<br \/>\nVersion of Record online: 15 MAR 2017<\/p>\n<p><a href=\"http:\/\/onlinelibrary.wiley.com\/doi\/10.1111\/maps.12841\/epdf\" target=\"_blank\"><strong>PDF (OPEN ACCESS)<\/strong><\/a><br \/>\n<a href=\"http:\/\/onlinelibrary.wiley.com\/doi\/10.1111\/maps.12841\/full\" target=\"_blank\"><strong>LINK (OPEN ACCESS)<\/strong><\/a><\/p>\n<p>&#8220;Metallic phases in the Tazewell IIICD iron and Esquel pallasite meteorites were examined using 57Fe synchrotron M\u00f6ssbauer spectroscopy. Spatial resolution of ~10\u201320 \u03bcm was achieved, together with high throughput, enabling individual spectra to be recorded in less than 1 h. Spectra were recorded every 5\u201310 \u03bcm, allowing phase fractions and hyperfine parameters to be traced along transects of key microstructural features. The main focus of the study was the transitional region between kamacite and plessite, known as the \u201ccloudy zone.\u201d Results confirm the presence of tetrataenite and antitaenite in the cloudy zone as its only components. However, both phases were also found in plessite, indicating that antitaenite is not restricted exclusively to the cloudy zone, as previously thought. The confirmation of paramagnetic antitaenite as the matrix phase of the cloudy zone contrasts with recent observations of a ferromagnetic matrix phase using X-ray photoemission electron spectroscopy. Possible explanations for the different results seen using these techniques are proposed.&#8221;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Blukis, R., R\u00fcffer, R., Chumakov, A. I. and Harrison, R. J. Meteorit Planet Sci. doi:10.1111\/maps.12841 Version of Record online: 15 MAR 2017 PDF (OPEN ACCESS) LINK (OPEN ACCESS) &#8220;Metallic phases in the Tazewell IIICD iron&#8230;<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[3496,214,810],"tags":[930,3500,1874,595,1894,3720],"_links":{"self":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/12057"}],"collection":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=12057"}],"version-history":[{"count":1,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/12057\/revisions"}],"predecessor-version":[{"id":12058,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/12057\/revisions\/12058"}],"wp:attachment":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=12057"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=12057"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=12057"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}